Dissected hydrologic system at the Grand Canyon: Interaction between deeply derived fluids and plateau aquifer waters in modern springs and travertine

@article{Crossey2006DissectedHS,
  title={Dissected hydrologic system at the Grand Canyon: Interaction between deeply derived fluids and plateau aquifer waters in modern springs and travertine},
  author={Laura J Crossey and Tobias P. Fischer and P. Jonathan Patchett and Karl E. Karlstrom and David R. Hilton and Dennis L. Newell and Peter W. Huntoon and Amanda C. Reynolds and G.A.M. de Leeuw},
  journal={Geology},
  year={2006},
  volume={34},
  pages={25-28}
}
Geochemical study of water and gas discharging from the deeply incised aquifer system at the Grand Canyon, Arizona, provides a paradigm for understanding complex groundwater mixing phenomena, and Quaternary travertines deposited from cool springs provide a paleohydrologic record of this mixing. Geochemical data show that springs have marked compositional variability: those associated with active travertine accumulations (deeply derived endogenic waters) are more saline, richer in CO2, and… 

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